2018
DOI: 10.2112/si85-029.1
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The Influence of Wind on Hydrodynamic Processes in Robbins Passage, Tasmania, Australia

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“…Furthermore, the higher biofouling coverage on the sporophytes at 1 m depth may have affected the performance as could drift seaweeds rubbed off on the growth lines near the surface (1 m), removing the kelp. Also, surface currents generated by wind (Nguyen et al 2018) may have removed sporophytes from the growth line before the holdfast developed enough for secure attachment. Similarly, Eisenia arborea cultivated in Baja California had fewer individuals at shallow (2-4 m) than deeper (7 -9 m) ropes (Zertuche-González et al 2022).…”
Section: At-sea Cultivation: Seasons and Depthsmentioning
confidence: 99%
“…Furthermore, the higher biofouling coverage on the sporophytes at 1 m depth may have affected the performance as could drift seaweeds rubbed off on the growth lines near the surface (1 m), removing the kelp. Also, surface currents generated by wind (Nguyen et al 2018) may have removed sporophytes from the growth line before the holdfast developed enough for secure attachment. Similarly, Eisenia arborea cultivated in Baja California had fewer individuals at shallow (2-4 m) than deeper (7 -9 m) ropes (Zertuche-González et al 2022).…”
Section: At-sea Cultivation: Seasons and Depthsmentioning
confidence: 99%
“…In the literature [1,2], the simulation of sea bottom changes produced by a coastal defence structure are usually carried out by simulating the hydrodynamic fields and the concentration of the suspended solid particles. In the framework of coastal sediment transport, 3D models for the simulation of the hydrodynamic fields [3][4][5][6] require considerable computational time, due to the long-time scale of the sea bottom variations.…”
Section: Introductionmentioning
confidence: 99%